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Avalanche Forecast

Archived

Dec 24th, 2017–Dec 25th, 2017

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

South Coast Inland.

It might not be much but it's better than a lump of coal! Looks like Santa's set to bring a dusting of new snow for Christmas morning. There may still be some lingering wind slabs to watch for, as well as more snow later in the week.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Light dusting (2-5 cm) of snow expected overnight Sunday and early Monday morning.MONDAY: Mix of sun and cloud, light flurries. Accumulation trace. Ridge wind light from the northwest. Temperature -9. Freezing level surface.TUESDAY: Mostly sunny. Ridge wind light from the southwest. Temperature -10. Freezing level surface.WEDNESDAY: Cloudy, light flurries. Accumulation trace. Ridge wind light to moderate from the west. Temperature -9. Freezing level surface.

Avalanche Summary

There have been no new reports of avalanches since last Wednesday when southern areas saw numerous loose dry to Size 1.5, as well as slab and glide avalanches to Size 2 on steep, leeward terrain and smooth rock slabs, while the northern part of the region reported wind slab activity up to size 2 on north and west aspects in the alpine.

Snowpack Summary

The recent storm snow has been redistributed by moderate to strong northerly winds in the alpine and exposed treeline areas, creating wind slabs in some areas and scouring others. The southern part of the region has seen impressive storm snow totals (80-100cm) since Sunday night, compared to northern areas of the region, which received 25-35cm. This new snow sits on crusts of variable thickness that formed on almost all aspects in mid-December (December 15th layer). On steep southerly aspects the crust is supportive, whereas on northerly aspects the crust is quite thin and variable. Beneath the December 15th layer the snowpack is well settled. The late November rain crust is now buried 50-80 cm in the northern part of the region and well over 1 m in the south. Great conditions reports from the north of the region are posted on the Mountain Information Network (MIN) here, as well as from the southern part of the region, here.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.